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简介：Althoughtheterraneconceptemergedfromthestudyofnorthernhemisphereactivecontinentalmarginsandorogenicbelts,itislargelyintheSouthernHemisphere,inparticularinrelationtotheGondwanasupercontinent,whereithasseenitsfullestflowering.Newdatacontinuetoemerge,andnewmodelsandtechniquesarebeingactivelydeveloped.Forthesereasons,“TerraneProcessesatthePacific-marginofGondwana”

简介：1.Introduction.ThelateMesozoicEastAsiancontincntalmarginwasamobilebeltsimilartorecentcontinentalares,buthadaconsidcrablcwidthmorcthan2,oookm’Thispapcrdcscribcstbegeometryofthemobilebc1t,anddiscusscsthckincmaticsanddynamics-Itwillclarifythatthermalp1umcundcrtbeEastAsiancontincntplaycdanhoportantrolei

简介：ThenorthernmarginoftheAlxablockisthejunctionofatectonicunits.Fourfirst-ordertectonicunitsaredistinguished:1.theYaganstructuralzonecharacteristicofanimmatureislandarc;2.theZhusileng-Hangwulastructuralzone,whichwasapassivecontinentalmarginintheEarlyPalaeozoicandwastransformedintoanactivecontinentalmarginintheLatePalaeozoic;3.theShalazhastructuralzonecharacteristicofamatureislandarc;4.theNuru-Langshanstructuralzone,whichwasaProterozoicorogenicbeltandlaterevolvedintoanextensionaltranstionalcrustinthePalaeozoic.Theabove-mentionedtectonicunitsdifferremarkablyinsedimentaryformations,magmaticrockassociations,metamorphismandgeochemistryandareboundedbyfaultsbetweenoneanother.

简介：MultistagesuperimposeddeformationhasbeendiscussedsystematicallybasedontheprogressofthestratigraphicsequencesofthenortheasternmarginofYangtzeBlock.Thenew-discoveredfirststagedeformationofthosesequencesoccurredfromthemiddleTriassictotheendofearlyJurassictogetherwithdevelopmentofregionalfolding,whichwasresultedfromthedeepdetachmentshearingtendingtowardNW-WNW.Thefoldsdiptoeastandfalldowntowardwest,andweresuperimposedbythemainstagefolding.Thereafter,aseriesoffoldsweredevelopedwithaxestrendingtowardnortheast.Consequentlynormalfoldsoccurredonthenormallimbswhileoverturnedfoldontheoverturnedlimbsduringthefirststagefolding.ThedetachmentorthrustwasformedfromlateJurassictoearlyCretaceous.DuetotheupliftingofDabieandtheWannanMountainsinthenorthandsouthsides,thebi-directionalthrustingbeltwasformedbygravityflowingfromtheMountainstowardthecenterofthebasinalongthenorthsideofXuanchengandsouthsideofGuichi.Thedeformationgeodynamicswasdiscussedsimplybasedonthenewlyrecognizedinformationaboutthetectonicevolution.

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简介：Asynthesisofcrustalthicknessestimateswasmaderecentlyutilizingavailablefield,geochemical,seismicity,shearwavevelocityandgravitydatainthePhilippines.TheresultsshowthatasignificantportionofthePhilippinearchipelagoisgenerallycharacterizedbycrustwithathicknessofaround25to30kilometers.However,twozones,whicharemadeupofathickercrust(from30to65km)havealsobeendelineated.TheLuzonCentralCordilleraregionischaracterizedbythickcrust.AnotherbeltofthickenedcrustisobservedintheBicol-Negros-Panay-CentralMindanaoregion.ThispaperexaminestheinterplayoftectonicandmagmaticprocessesandtheirroleinmodifyingPhilippinearccrust.Theprocesses,whichcouldaccountfortheobservedcrustalthicknesses,arepresented.Thecontributionsofmagmaticarcsascomparedtothecontributionoftheemplacementandaccretionofophiolitecomplexestocrustalthicknessarealsodiscussed.

简介：学习的水属于温暖(T=30-50°C)，碱(pH=8.9-9.3)，低使矿物化(TDS<235mg/l)Na-HCO3或Na这样有高度的热水SiO2(多达81mg/l)满足的4-HCO3和F(多达3.9mg/l)，在东方Sikhote-Alinorogenic带的现代火山构造的恢复区域上发生。低3他集中以及N2/O2和N2/Ar比率排除深披风液体的影响。新稀土元素元素数据抑制我们水岩石相互作用发生在水来源区域的理解。水的大气的起源被从−71‰变化的稳定的同位素价值证明到−136.1‰并且从−10.8‰到−18.8‰为δ2H和δ18O分别地。REE模式反映高pH，从水岩石相互作用的resultfing和氧化条件。用Na-K和石英地温计的深含水土层温度的计算分别地显示出116.8-131.1°C和82.2-125.8°C。深差错的存在两个与反常热坡度(∼45-50K/km)定义Sikhote-Alin的热水的唯一的geochemical形状，区域，在没有现在的暴烈的活动被登记的地方。

简介：<正>TheDevonianhydrotyermalsedimentationandmineralizationarewidespreadandtypicalinMaizi、KelangandChonghuerbasinsofsouthernAltaymargin,andhavetheirrespectivesignsinoccurrence,fabricandgeochemistry.Hydr)thermalsedimentaryrocksmainlyoccurintheintermittentperiodbetweenvolcanicsub(?)ycles.Theyarethin-midium-bedded,lenticularandbasicallyuniformtotheoccurrencesoftheoverlyingandunderlyingstrata.Theclassificationofthehydrothermalsedimentaryrocksisproposedbasedonthemineralcompositions.Thedetaileddescriptionsaregiventothefivetypesofhydrothermalsedimentaryrocks:silicates,feldspar-richrocks,

简介：Themarginofappreciationiscontroversialanddifficulttounderstand.SinceitsfirstreferenceinthecaseofGreecevs.UK,themeaningofthisdoctrinehasevolvedfromdeferencetoderogationfromtheEuropeanConventiontoaninflationoflanguageusedormisusedbytheStrasbourgCourttopreservetheState’s"roomformanoeuvre"or"latitudeofdeferenceorerror."Inthispaper,Idividetheconceptofmarginofappreciationintotwocategories:thesubstantiveandstructuralconcept.TheStrasbourgCourtusuallygenerouslydeferstonationaldecisionsinstructuralscrutinywhereithastorespectEuropeanpluralismandthecollectiveinterestsofthecontractingpartiesunlessdomesticdecisionsareregardedas"manifestlyunreasonable."Incontrast,theEuropeanHumanRightsCourtscrutinizescarefullyinthesubstantivesenseofmarginofappreciation.Somefactorsortestapproacheswillbeidentifiedfirst,bywhichtheCourtsubstantivelynarrowsorlimitsthescopeofmarginpreservedfortheStates.Theresultoftwoconceptualmarginsofappreciationmaybereciprocallytransformedinsomecircumstances.WhenthecollectivegoodsurelyunderminesthecoreofConventionrights,theCourtwillnotstandwiththedomesticargumentsinceitmustensuretheimplementationofpan-Europeanhumanrightsstandards.Ontheotherside,theCourthasnocapacitytofurtherincreasestrictscrutinyincaseswherethereisacomplicatedrelationshipbetweenthemeansandendsintheproportionalitytest,implyingthatdomesticcourtsarebetterplacedthanthesupranationalcourtgiventhefactthattheyknowbetterthelocalrealityandhavemorelocalknowledge.

简介：ThecontinentalmarginalextensionconceptdevelopedbyChinesegeologistsrecentlymaybeappliedtotheexplanationabouttheCenozoicextensionanddivergentmovementoftheEasternAsiancontinentalmargin.Fromtheviewpointofcontinentalmarginalextension,thispaperdiscussesthedeeptectonothermalmechanismofthetectonicextensionoftheEasternAsiancontinentalmargin.TheEasternAsiancontinentalmarginisanextensionalbeltwithintensivemagmatismandstructuraldeformation,geophysicallycharacterizedbycontinualearthquakesandobviousgeothermalanomaly.SeismictomographicalresultsabouttheEasternAsiancontinentalmarginimplythatthePacificPlateissubductedtowardtheEurasianPlateatalowangleandthedivingPacificPlateliesonthesurfaceofthe670-kmphasetransitionalzone.Weinterpretthisfeaturetoberesultedfromretrogressivesubductionfollowedbycontinentalmarginalextension.Ourthermalmodelingandgeodynamicalcomputationresultssuggestthattheretrogressivesubductionoccurredatabout76Maandthewithdrawalofthetrenchservedtosupplythevolumeforthecontinentalgrowth,whichledtotheformationofthegrowingfrontoftheEasternAsiancontinentalmargin.ThegrowthwidthoftheEasternAsiancontinentalmarginisabout700km.

简介：Inthispaper,wecalculatedmulti-scaleresidualgeoidanomalieswiththemethodofgeoidseparationprocessing,accordingtoEGM2008ultra-highordergravityfieldmodel,remove-restoretechniqueandStokesintegral.TheEastAsiancontinentalmarginwasselectedasthestudyarea.Theresidualgeoidanomalieshavebeencalculatedbyprogramming.Onthebasisofresidualgeoidanomaliesatvariousorders,theinterlayergeoidanomaliesatdifferentdepthswerecalculatedtodepictthespatialdistributioncharacteristicsoftheresidualgeoid.Finally,weconductedadetailedgeophysicalinterpretationforthestudyareaaccordingtothegeoidanomaliesincombinationwithothergeophysicaldatasets.Fourconclusionscanbeoutlinedasfollows：1）itisimpracticablethatgeoidanomaliesareusedintheinterpretationoftheshallowobjectsduetotheinfluenceoftheterrain;2）theanomaliesofresidualgeoidcanreflecttheintensityofsmall-scalemantleconvectionintheasthenosphere;3）theinterlayergeoidanomaliescanreflectthemagmaticactivitiesassociatedwiththemantleconvectionandmantleplumeindifferentscales;4）thestudyofthegeoidmayprovideanapproachfortheresearchofthesubductionzone,mantleconvectionandmantleplume.

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简介：Theformationofstrathandstrathterraceiscloselyrelatedtotectonicupliftinthedrainagebasin.BasedontheinvestigationofstrathsatYandantuandChangcaogouontheeasternsegmentofthenorthernmarginfaultofAltun,andincombinationwiththepaleoclimaticdata,thetectonicupliftsincelateEpipleistoceneasrevealedbystreamterracesatthetwoplacesisdiscussed.AtYandantu,threelevelsofstreamterraces(T1,T2andT3)havedevelopedsince16kaBP,whereT1,T3andT2arefillterracesandtheburiedmajorstrathsareexposed.Theagesofthreetreadsaredatedtobeabout16.1kaBP,12.8kaBPand6.2kaBP,respectively.Thethreeterracesreflectthreetectonicupliftevents,whiletheagesofthetreadsrepresenttheoccurrencetimeoftheseevents.Thestreamisstillbevelingthebedrockandwideningthechannelatpresent,andthemodernstrathisbeinggenerated.Theupliftrateis4.8～4.5mm/asince16.1kaBPinthisarea.From12.8kaB.Pto6.2kaBP,Theupliftratewas6.4mm/a.Theupliftrateis3.1mm/asince6.2kaBP.AtChangcaogou,fourlevelsofstreamterraces(T1,T2,T3andT1′)havedevelopedsince7kaBP.Allofthemarefillterraces.Thereareburiedstrathsunderthedeposits.TheburiedmajorstrathisexposedonT3andT2andtheminorstrathonT1′andT1.Theagesoftreadsofthethreeterraces(T3,T2andT1′)are7kaBP,3kaBPand2.5kaBP,respectively.Thefourterracesreflecttwouplifteventsinducedbytectonicactivities.Oneoccurredinabout7kaBP,andtheotherin3kaBP.Theupliftrateis5.9mm/asince7.0kaBPatChangcaogou.From7kaBPto3kaBP,theupliftratewas7.0mm/a,andsince3kaBPtillnow,theupliftrateis4.7mm/a.

简介：<正>EXTENSIONOFTHECATHAYSIANDIWA-TYPEOROGENSANDCONTINENTALMARGINSPREADINGINSOUTHEASTCHINAZouHeping(DepartmentofGeology,ZhongshanUniversity,Guangzhou,510275,China)lateorogenicextension,Diwa,crustobody,continental-margin-spreading,SoutheastChina.Adynamicmechanism,"lowerlithosphericdelaminationandextensionoftheCathaysianDiwa-typeorogens",hasbeenputforwardtoexplaintheformationoftheCenozoiccontinental-margin-spreading-beltinSoutheastChina.Theprocessesofformationanddevelop-mentforthebeltarefromthestageoftheCathaysianDiwa-typeorogensatwhichcompressionandthickeningofcurstobodiesprevailed,tothestageofthebasin-and-range-typestructuresatwhichthelateorogeniccrustalextensionoccurred,andthentothestageoftheepicontinentalDiwa-typeriftsatwhichthelithosphericextensiontookplace.

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简介：Eolian灰尘免职是亲密地与大气的循环和来源区域的环境背景有关，并且因此是为学习大气的发行量模式和paleoclimatic变化的进化历史的一个无价的工具。识别任何eolian存款的起源为重建是关键的不仅灰尘来源区域的paleoenvironmental历史，而且为理解各种各样的索引的paleoclimatic意义。从西藏的高原(TP)的东方边缘上的Garze区域的黄土和paleosol样品被分析为他们的元素(专业和踪迹元素)并且同位素(Sm-Nd)地球化学并且与那些相比，北汉语(NC)，黄土在一样的年龄形成了。结果证明Garze黄土和paleosol样品的geochemical作文类似于中国黄土高原(CLP)上的那些eolian存款，并且也类似于平均UCC。这显示TP的东方边缘上的eolian存款从经历了众多的上面的外壳的再循环过程的混合得好的沉积protoliths被导出，就就象CLP黄土存款。与NC黄土相比，然而，Garze样品有更高的ΣREE，李，Rb，Zr，C，Hf和双性人集中，更高的TiO2/Al2O3,Hf/Nb，La/Nb，Th/Nb和更低的K2O/TiO2,Zr/Hf，Ba/Rb比率。从Sm-Nd同位素的地球化学，εNd(0)和147Sm/144Garze黄土和paleosol样品的Nd价值清楚地比NC黄土低。，更高级的双性人，Zr和Hf集中与在这个区域的广泛地分布式的acid-magmatic岩石相关李，的更高的内容C，Rb被归因于TP的高背景价值。Garze黄土和paleosol的geochemical特征进一步取样证明冰川的本地人和另外的第四级的由岩屑形成的沉积是主要为TP的东方边缘上的eolian存款的贡献者。在在不同时间形成的Garze黄土和paleosol样品的稳定的元素集中和他们的比率与NC黄土比较有相对更大的变化范围，显示自从晚早的更新世，为eolian存款的来源区域是不稳定的。我们与TP的uplift

简介：云南的广泛的Eshan花岗石由他们的地接触关系区分的三个恼人的单位组成；在下年龄的顺序，他们是Pojiao单位，L吗？？

简介：TheeasternmarginofTibetanPlateauisoneofthemostactivezonesoftectonicdeformationandseismicityinChina.Tomonitorstrainbuildupandbenefitseismicriskassessment,weconstructed14survey-modeglobalpositionsystem(GPS)stationsthroughoutthenorthwestofLongmenshanfault.AnewGPSfieldover1999–2011isderivedfrommeasurementsofthenewlybuiltandpre-existingstationsinthisregion.Sequentially,twostrainratefields,oneprecedingandtheotherfollowingthe2008MW7.9Wenchuanearthquake,areobtainedusingtheGausianweightingapproach.Strainfieldover1999–2007showsdistinctstrainpartitioningpriortothe2008MW7.9Wenchuanearthquake,withcompressionspreadingoveraroundLongmenshanarea.Strainfieldderivedfromthetwomeasurementsin2009and2011showsthattheareaaroundLongmenshancontinuestobeunderstrikingcompression,asthepatternprecedingtheWenchuanearthquake,implyingacausativefactorofthesequentof2013MW6.7Lushanearthquake.OurGPSderiveddilatationshowsthatboththeWenchuanandLushanearthquakesoccurredwithinthedomainofpronouncedcontraction.TheGPSvelocitiesdemonstratethattheLongribafaultunderwentslightmotionwiththefaultnormaland-parallelratesat1.0±2.5mmand0.3±2.2mm/a;theLongmenshanfaultdisplayedslowactivity,withafault-normalrateat0.8±2.5mm/a,andafault-parallelrateat1.8±1.7mm/a.LongribafaultisonaparwithLongmenshanfaultinstrainpartitioningtoaccommodatethesoutheastwardmotionofeasternmarginoftheTibetanPlateau.Integratedanalysisofprincipalstraintensors,meanprincipalstress,andfastdirectionsofmantleanisotropyshowsthatwestofSichuanischaracterizedasmechanicallystrongcrust-mantlecoupling.更多还原